catalogo de terremotos para america del sur catalog of earthquakes ...

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158 APPENDIX A (Continued) Columns Heading Sub-heading Description 17-54 LONG Longitude (listed to thousandths of a degree, but not necossarily accurate to that level.) Negative values indicate west longitudes. 56 QUAL Code used to indicate the quality of 58-63 DEPTH the epicenter (see table 2). 58-62 KMS Focal depth in kilometers (listed to the nearest tenth of a kilometer, but not necessarily accurate to that level). 63 QUAL Code used to indicate the accuracy of the depth (see table 3). 65-67 NUM STA Number of stations used in the hypocenter computation. 69-71 HYP SRC CODE Hypocentral data source (see table 4). 73-79 m b Body-wave magnitude estimate, if available. Different sources may vary significantly in the method used to compute mb-magnitudes. References describing the method of magnitude computation are given in table 5. 73-75 MAG Magnitude value, given to the nearest tenth of a unit. 77-79 SOURCE Three-letter code indicating the magnitude sGzrce (see table 5). 81-88 MS Surface-wave magnitude estimate, if available. Table 5 gives references which describe the computation of these magnlttvdes. 81-83 MAG Magnitude value given to the nearest tenth of a unit. 84 COMP Seismogram component used for the magnitude determination. H indicates the horizontal component and Z Indicates the vertical component.
APPEYN X A (Continued) Columns Headi ng Sub-headi ng Description 86-88 SOURCE 'lhree-letter code indicating the magn tidc sourco (see table 5). 90-106 OTHER MAGNITUDES Thin section at I w!; space to lit two add iti ,onal may:W,, ent;, , If available. The'se may be add1tio; l estimates of m or M. magni ud,,: they may be magn itud,. from a Iifr'(ent, i ': , q as momentimlagn i tiidea , or thay may ibu magni t;ld(:.3 baned on a conver: ton from intensity data or' from one maignitide scale to another. 90-92 MAG Magitl ude valwoo, g i veni to the nearest tenth of a unlt. 93 SCALE Single-letter' code ind icatin g the nagnitude a cae or conversion relationship (ne table 6). 95-97 SOURCE Three-letter code indicating the magnitu de source (ace table 5). 99-101 MAG Magnituide value, given to the nearest tenth of a unit. 102 SCALE lingle-letot,,r node Indicating the magn-tud ', :3ca l op' conver'.sion reiationship (see table 6). 104-106 SOURCE Threo-.let tar code iadiIca.;I, og the magnitude soirce (nee tabe 5). 108 110 FOG MEC SOURCE Focal mechanism soure (oac table 4). 112-120 INTENSITY 112 DATA An * in this column Indicates detailed Intensity data are available for this event ir the intersity catalog. 114-115 MAXINT Estimate of the maximum ineni ty 1inted I n d, I-_ Ia a, .' ,r1' . 116 SCALE Si ngl e--I etter' code ndlcat ng the: Intensity soca mIoo rj for the maximum Intensi ty eL imate. An M indicates the Modified Mercalili scale, and a K MYdicates the NSK scale.
Page 1 and 2:
Centro Regional de Sismologfa para
Page 3 and 4:
Este trabajo se publica con el ente
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INDICE - CONTENTS DESCRIPCION DEL C
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Pals Coordinador Investigadores 2 R
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'4 Todas Ias intensidades 1istndas
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individuales. Esto requiriA definir
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8 mb = log (A/T) + 1.35 log (A ) +
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10 Modificada o MSK. El investigado
Page 17 and 18:
Conclusiones 12 Los catilogos unifi
Page 19 and 20:
Introducci6n 15 CATALOGO DE TERREMO
Page 21 and 22:
17 Los criterios de selecci6n de ev
Page 23 and 24:
4. Torremoto Stdin .i Cl ino del 3)
Page 25 and 26:
INTRODUCCION CATALOG(O DE TE KREMOT
Page 27 and 28:
23 A 0 ML = lig A/T + 1.9 log + 3.5
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25 A partir de 1982 los datas sismi
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27 m) = 1.63 + 0.60 Jog (At), 6 i b
Page 33 and 34:
29 SADOWSKI, G.R.; CSORDAS, S.M. &
Page 35 and 36:
A Ia colmna 131 (WFn6munus s -t , n
Page 37 and 38:
3 KAUSEI,, E. (1979d). Terremoto do
Page 39 and 40:
INTRODUCCION .'5 CATAIO(;O DE .1ElI
Page 41 and 42:
37 se pretendla adem~s elaborar lis
Page 43 and 44:
eA. arclivo del InS.-LAtti) (eolisi
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ESt'ASA-CAI.I'.- ,i, r'pvdia Uni v.
Page 47 and 48:
INTRODUCCION I. Investigadores clab
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7. Io t ermi i (i ojliiao s i dad !
Page 51 and 52:
INTRODUCC1ON 47 CA'ALOOI ) I)t.E TF
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4Q) ciertos recientes evento:s gi a
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INTRODUCCION CATALOGO DiE TEi,;RNI,
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la interpretaci6n de descripciones
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fuente du a"lorl;a B; (tp ignaJ~l m
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)'''n4'Va,!o "IN't; MK3, n importtn
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59 I so ejemplifican algunos tomado
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a"lt or i6 at Ias' primrdB JleM ros
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DESCRIPCION DIE ENT RADA.; IV,N , C
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APFICE1 f A (CihnL inaari 'Si) (>I
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APENDICE A (Continuacj6n) Columna r
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APENDICE B (Continu cin) Co ,,_ i t
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Tipa do Hlypocent:ro V.digo SISRA T
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' ipo de Cd igo Ilypocentro STSRA n
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71, EGR Egred, J., 1M8, Breve hiq;t
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77 Colombia y en la Cuenca d la Ama
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'FAiLA 5 - tCHDI T ,IA W FUENK:TES
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TAG Uniiye rsia IN(( N;wci on.i (.'
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83 TABLA 7 - INTtERPRETES APO Oscar
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711 No not nd. ,.a(~ i n V-npz;o Ia
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x / TABA F.- K Fi! N(:IAS 101 Infor
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31i3 lescotes, P.M., and Cahr,', Gc
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422 Polo, J.T., 1904, Sinopsis do t
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P.114411 > .iII, 11.Ci'144 1 P . ,
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9 5 REFI EN(CI AS CITADAS Bath, M.,
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Introducti on 97 SOUTH AMERICAN HYP
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99' Country Coordinator Investigato
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101 is provided for four, magnitude
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S03 These bulletins, for the time s
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locally which actually fell in Colc
Page 111 and 112: Brazil: Magn!tudes (mb) were comput
Page 113 and 114: intensities but also the distributi
Page 115 and 116: assigned the iJntonnsity value is a
Page 117 and 118: Shallow: 0-70 kms. S11 Intermediate
Page 119 and 120: 115 compiled, is to more clearly de
Page 121 and 122: INTRODUCTION 117 CATALOG OF EARTHQU
Page 123 and 124: I 9 The criteria for tbe selection
Page 125 and 126: 121 Mendoza: Vil].a Atucl and las t
Page 127 and 128: INTRODUCTION 123 CATALOG OF EARTHQU
Page 129 and 130: 125 M = 1.08 + 0.62 fmx 2. Intensit
Page 131 and 132: 127 and Sternberg (1953) who compil
Page 133 and 134: 129 mb = 1.63 + 0.60 log(A t), or m
Page 135 and 136: INTRODUCT I ON 131 CATALOC OF EARTI
Page 137 and 138: INTRODUCTION 133 CATALOG OF EARTHQL
Page 139 and 140: 1.35 later investigation and for th
Page 141 and 142: t lh, l .'a lua11t-io ,Fi i- t ii.
Page 143 and 144: 1NTRODUCT ION 1. Participating: 139
Page 145 and 146: 7. l)eterminat ion of inten, it rie
Page 147 and 148: ]1 3 sources that appear i the refe
Page 149 and 150: informna tion. For pl;.ce: who.o i
Page 151 and 152: 47 in thu conmpiliation presunted a
Page 153 and 154: ii) Every evnl or : Bra:zeo, and fo
Page 155 and 156: is adopted. where: 151 From the equ
Page 157 and 158: 153 TAB IF N ° INTENSITY OBSERVATI
Page 159 and 160: V n u la (1971; 107'); The 'imes At
Page 161: 11 / A 1'P!' I')IX A DESCIIlPTION O
Page 165 and 166: 1,1 APPENDTX A (Continued) Columns
Page 167 and 168: I 63 APPENUITX 11 (Continued) Colum
Page 169 and 170: Type of' Hyuoeenter I n 3 t r u m e
Page 171 and 172: 10 7 TABLE 3--.DEPT!H QUALITY FACTO
Page 173 and 174: 'rAILE 4--(Contlnued) EDR Earthquak
Page 175 and 176: i I I TABLE 4--- (Continued) MOL Mo
Page 177 and 178: TABLE 4--(Continued) Wt3 Bachmann,
Page 179 and 180: t 75 TABLE 5--Continued JGG Grases,
Page 181 and 182: I i7/ TABLE 6--MAGNITUDE SCALE CODE
Page 183 and 184: IILBV P. liuaco, W. Lescano, A. Buo
Page 185 and 186: TRMl Trinidad Station, Trinidad, We
Page 187 and 188: 211 larrington, I.j., 1944, Volcano
Page 189 and 190: 185 405 1952, Rmto!; s i,,ivoi 6 gi
Page 191 and 192: 187 436 Espejo, G., y fluaco," P.,
Page 193 and 194: I8H9 916 "'El Naciuta'l", (Pt ri 1i
Page 195:
191 Needham, R., ard Steele, A., 19
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